@Article{VeigaNGCSCSKFBMRBON:2023:ClChOv,
author = "Veiga, Sandro F. and Nobre, Paulo and Giarolla, Emanuel and
Capistrano, Vinicius B. and Silva J{\'u}nior, Manuel Baptista da
and Casagrande, Fernanda and Soares, Helena Cachanhuk and Kubota,
Paulo Yoshio and Figueroa, Silvio Nilo and Bottino, Marcus Jorge
and Malagutti, Marta and Reyes Fernandez, Julio Pablo and Bonatti,
Jos{\'e} Paulo and Oliveira, Gilvan Sampaio de and Nobre, Carlos
Afonso",
affiliation = "{Nanjing University} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Universidade Federal de Mato Grosso do Sul (UFMS)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade de S{\~a}o Paulo (USP)}",
title = "Climate change over South America simulated by the Brazilian Earth
system model under RCP4.5 and RCP8.5 scenarios",
journal = "Journal of South American Earth Sciences",
year = "2023",
volume = "0,0",
pages = "e104598",
month = "Nov.",
keywords = "BESM2.5, Climate change, Extremes, Precipitation, South America,
Surface air temperature.",
abstract = "Climate projections simulated by the Brazilian Earth System Model
(BESM2.5) under RCP4.5 and RCP8.5 climate scenarios are analyzed
based on future changes of surface air temperature (SAT) and
precipitation with respect to the historical reference period
19712000. Since BESM2.5 is the only climate model developed in a
South American country, this study gives a particular emphasis to
South American future climate projections. Regarding the surface
air temperature, BESM2.5 projects a steady warming throughout the
21st century, with the highest warming over eastern Amazonia,
northern Chile and central South America for both scenarios. The
SAT changes range between 2 °C and 34 °C for RCP4.5 and RCP8.5,
respectively. On the other hand, projected precipitation varies
over different regions of South America, with decreasing and
increasing trends over the Amazon and southern South America,
respectively. Interestingly, this study shows contrasting results
with respect to extreme precipitation indicators, projecting
enhanced extreme events with higher numbers of both consecutive
dry days and days in which the precipitation exceeds 20 mm over
the southeastern region. The model projects a meridional dipole
pattern in the precipitation, with decreasing precipitation and
longer dry spells over Northeast Brazil and the East Amazon region
and increasing precipitation and shorter dry spells over Northwest
South America and West Amazon, that is driven by future changes in
the SLP that imposes a meridional gradient over these regions,
causing the increase of westerlies that are likely to increase the
moisture transport from the Pacific Ocean into western South
America and the weakening of the easterlies that transport
moisture over eastern South America and East Amazon.",
doi = "10.1016/j.jsames.2023.104598",
url = "http://dx.doi.org/10.1016/j.jsames.2023.104598",
issn = "0895-9811",
language = "en",
targetfile = "1-s2.0-S0895981123004108-main.pdf",
urlaccessdate = "29 jun. 2024"
}